19 Chikyū

drill ship docked in port
JAMSTEC (Japan Agency for Marine-Earth Science and Technology)’s deep-sea drilling vessel Chikyū. Photo taken at Yokosuka New Port, Kanagawa, Japan (2005). From Wikimedia Commons.

 

Chikyū is currently the largest scientific drilling vessel. Built in 2005, what makes Chikyū different from other drilling vessels is its ability to drill 7,000 meters below the seafloor through its riser drilling technology. The Japan Agency for Marine-Earth Science and Technology (JAMSTEC) owns Chikyū, with the ship operated by its Centre for Deep Earth Research (CDEX). Chikyū’s mission includes:

  • Understanding marine disasters
  • Elucidating the global climate and ocean changes
  • Understanding the subseafloor biosphere

 

Riser drilling technology

What is a riser drilling system? View this video to learn how the drilling process is carried out deep below the seafloor.

Exercise – A quick check on your knowledge of riser drilling

To ensure your understanding of a riser drilling system, how would you respond to these questions:

  • Why is drilling mud used instead of seawater in a riser drilling system? What are the advantages?
  • Why is drilling mud reused? How is used drilling mud collected?
  • What is done to ensure a drilled hole does not collapse?

 

To continue to understand the full drilling process of Chikyū, continue by viewing this video.

 

As part of the Integrated Ocean Drilling Program (IODP, 2003-2013) and International Ocean Discovery Program (IODP, 2013-2024), Chikyū completed 18 expeditions (through EXP 380), visiting 44 sites and recovering 5,978 meters of core material. The deepest water depth Chikyū has drilled as part of IODP was 6,929 m, and its deepest hole penetrated was 3,059 m.

 

SciOD Spotlight – The Boarding Process with Jon Lewis

Person standing on a ship wearing a hardhat and work coveralls
Jon Lewis on Chikyū (2007). Image provided by J. Lewis.

Before scientists are allowed to board Chikyū, there is mandatory safety training that must be completed. Jon Lewis sailed on Expedition 315, which required him to board the ship from helicopter on to the ship’s helipad. Take a listen to Jon describing what was involved, and why he thought he might not pass the training.

 


 

Although the majority of us will never have the opportunity to step foot on Chikyū (or land on Chikyū, as Jon did), you can come very close to a model of the ship. If you find yourself one day visiting Washington DC, enter the Sant Ocean Hall at the Smithsonian Institution National Museum of Natural History. Here, you will see a 1:100 scale model of Chikyū and be able to learn more about scientific ocean drilling as well as what we can learn from deep-sea mud and sediment.

Gallery of images in the Sant Ocean Hall of the Smithsonian’s Natural History Museum. Images taken by L. Guertin (CC BY 4.0).

 

Learn about a Chikyū expedition!

This four-part video (~30 minutes in total) follows Expedition 365, Exploring the Fault Trace, which sailed March 26 – April 27, 2016. As you watch the video, how would you respond to the following questions? Note that some of these questions have additional information presented in different sections of the video.

 

  • What are the scientific objectives of this expedition? Why is Chikyū at the Nanki trough?
  • For this expedition, microbiologists were on board. What are scientists hoping to learn about the subsurface biosphere, and how was Chikyū involved in getting this material for the scientists?
  • What is the technology being used to accomplish the scientific objectives?
    • What type of information can be retrieved from long-term borehole monitoring systems?
  • How will the scientific results of this research benefit society, not just in Japan but globally?
  • State a maximum of three points during this video where you had an “ah-ha” or “wow” moment. What made these items you viewed stand out to you?

 

 

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Scientific Ocean Drilling: Exploration and Discovery through Time Copyright © 2024 by Laura Guertin; Elizabeth Doyle; and Tessa Peixoto is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, except where otherwise noted.

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